Development of crystal orientation fabric in the Dome Fuji ice core in East Antarctica: implications for the deformation regime in ice sheets

Abstract

The crystal orientation fabric (COF) of a polar ice sheet has a significant effect on the rheology of the ice sheet. With the aim of better understanding the deformation regime of ice sheets, the work presented here investigates the COF in the upper 80% of the Dome Fuji Station ice core in East Antarctica. Dielectric anisotropy (δϵ) data were acquired as a novel indicator of the vertical clustering of COF resulting from vertical compressional strain within the dome. The δϵ values were found to exhibit a general increase with depth, but with fluctuations over distances in the order of 10-102m. In addition, significant decreases in δϵ were found to be associated with depths corresponding to three major glacial to interglacial transitions. These changes in δϵ are ascribed to variations in the deformational history caused by dislocation motion occurring from near-surface depths to deeper layers. Fluctuations in δϵ over distances of less than 0.5m exhibited a strong inverse correlation with δϵ at depths greater than approximately 1200m, indicating that they were enhanced during the glacial-interglacial transitions. The δϵ data also exhibited a positive correlation with the concentration of chloride ions and an inverse correlation with the amount of dust particles in the ice core at greater depths corresponding to decreases in the degree of c axis clustering. Finally, we found that fluctuations in δϵ persisted to approximately 80% of the total depth of the ice sheet. These data suggest that the factors determining the deformation of ice include the concentration of chloride ions and the amount of dust particles, and that the layered contrast associated with the COF is preserved all the way from the near-surface to a depth corresponding to approximately 80% of the thickness of the ice sheet. These findings provide important implications regarding further development of the COF under the various stress-strain configurations that the ice will experience in the deepest region, approximately 20% of the total depth from the ice/bed interface.